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Title
Texas lignite : near-surface and deep-basin resources
Publisher
University of Texas at Austin. Bureau of Economic Geology
Series
Report of investigations (University of Texas at Austin. Bureau of Economic Geology) Volume no. 79
Date
1974
Author
Kaiser, W. R.

17

Simsboro marks the culmination of a major pro gradational or regressive phase which began in the lower Hooper Formation. Note the multistacking of coarsening-upward, progradational delta-front sequences in the Hooper (fig. 15). The thin and discontinuous nature of the Hooper lignites is readily explained in terms of accumulation as interdistributary peats during active deltation or progradation. Following Simsboro deposition sedi mentation slowed and on foundering older deltas, extensive lignites accumulated as delta-plain blanket peats during lower Calvert Bluff deposi tion. These are the lignites being strip-mined at Big Brown near Fairfield and Alcoa in Milam County. The sedimentology of the remainder of the Calvert Bluff is not clear. In the Bastrop County and Leon County areas the lignite sequence (delta-plain deposits) appears, based on electric-log patterns, to be overlain by distributary channel deposits and/or

delta-front sequences (fig. 15). The latter signal the start in the upper Calvert Bluff of a second major progradational phase. Deltaic deposition closes the Wilcox which is, in turn, in outcrop uncon formably overlain by braided stream deposits of the Carrizo Sand (Claiborne Group).

Potential lignite deposits (table 3) are shown on figure 7. They have been outlined with regard to inferred stratigraphic occurrence in the lower Calvert Bluff Formation, reported outcrop and well occurrences (Dumble, 1892; Fisher, 1963), and projection from deep-basin occurrences. The value of the latter as a clue to near-surface occurrences is well illustrated in figure 7. Note the fingerlike projection in eastern Bastrop County pointing updip to the Sayersville-Bastrop district, an important old mining district. Another similar projection in western Houston County points

Table 2 (continued)—

County

Group or Formation

i Location

Thickness 1 (feet)

Facies

Panola

Wilcox

northwestern part; Beckville area (site of Industrial Generating Co. strip mine)

5-15

fluvial

Rains

upper Wilcox

southeastern part; vicinity of Ginger

3-10

fluvial

Robertson

Calvert Bluff

west-central part north of Calvert in general

3-12

deltaic

area of Brazos River; Little Brazos River and

Walnut Creek

Shelby

Wilcox

vicinity of Timpson and Stockman

4-6.5

lagoonal

Titus

Wilcox

southern half; vicinity of Winfield (site of

4-11

fluvial

Industrial Generating Co. strip mine),

Mt. Pleasant, CookviHe

Uvalde

Indio

southeastern part; east of Leona River to

5-10

lagoonal

west of Nueces River

Van Zandt

Wilcox

Canton and Edgewood areas

5-12

fluvial

Wood

Wilcox

extreme western edge; Alba-Hoyt district

8-13

fluvial

Zavala

Indio

northwestern part; astride the Nueces River

3-10

lagoonal